Previous Page  154 / 218 Next Page
Information
Show Menu
Previous Page 154 / 218 Next Page
Page Background

[

] 152

S

URROUNDED BY THE

Alpine mountains to the west, and

the Carpathian mountains to the north and east Hungary’s

basin situation is accompanied by several long and short-

term weather extremities despite its temperate climate, which

is accredited to its 46-48 N geographical latitude. Four such

extreme events are droughts, heat waves, vast local precipita-

tion (flash-floods) and convective windstorms. By looking at

the phenomenology and regional characteristics of these

events, it will be possible to point to the relevant services

provided in each case by the National Meteorological Service

(NMS), including forecasts and warnings of the event.

The phenomena are listed in decreasing order of their time

scales. Hence, the possibility and importance of forecasting

(i.e. the factor of timely warning) rapidly increases, whereas

our ability to judge more recent and future trends, diminishes.

Drought

Hungary is situated in the Carpathian basin, surrounded by

mountains but open to the south. This geographical position

can also contribute to the fact that precipitation tendencies in

Hungary are similar to those in the Mediterranean region. In

addition, the largest decrease of precipitation can be found in

the more humid areas. Therefore, almost the whole territory

of the country suffers from water scarcity, mostly through

frequent drought events.

Monthly precipitation can reach 200 millimetres in almost

any month and region, but months without a drop of precipita-

tion may also occur in any season. Sometimes both flood and

drought are experienced in the same region during the same

year. Annual and seasonal precipitation amounts are decreasing,

with one exception. The summer precipitation totals have no

definite trend themselves, but the water management situation

is still worsening, as precipitation occurs in fewer cases and with

higher intensity. Besides this inconvenient dosage of precipita-

tion, positive temperature trends also intensify the problem.

The average situation is well characterized by the temporal

evolution of annual minima and maxima of the Palmer

Drought Severity Indices (PDSI) in Debrecen. Both the annual

maxima and minima have a decreasing tendency, indicating an

increasingly large chance of droughts. Debrecen is situated in

the north-east region of Hungary. From among the three typical

climats that influence Hungary (oceanic, Mediterranean and

continental), the climate of Debrecen is mainly governed by

the latter.

The Hungarian Meteorological Service (HMS) operates an

interactive irrigation advisory system through its homepage,

free of charge

(www.met.hu

). The irrigation model uses the

observed data of precipitation and plant-specific, estimated

evapotranspiration, all obtained from automatic weather

stations to describe the actual plant water demand.

Heat waves

The mean summer temperature was 19.6 degrees Celsius in the

1961-1990 normal period. Since its end, however, both the average

and the deviations from it seem to have changed significantly.

Parallel to global warming, the simple linear trend of the summer

Battling extreme weather under

a temperate climate – Hungary

Gyuró, Gy., Á. Horváth, M. Lakatos, S. Szalai and J. Mika, Hungarian Meteorological Service

Change in annual precipitation (%) in Hungary for the period

1951-2004. Exponential trend estimation is applied, and the

results relate to the 54-year long interval

Source: OMSZ

Severe weather warning for 20 August 2007, issued at 17:38 UTC

for the official website of the Hungarian Meteorological Service

Source: OMSZ